Abstract
An analysis of a number of samples from the Tomtor deposit of Nb and rare-earth elements (Republic of Saha (Yakutia)) by X-ray diffractometry, IR spectroscopy, and Raman spectroscopy makes it possible to cover the structural organization of minerals and their components from the long-range to the mid- and short-range orders. The apatites present in the samples are characterized by a large variety of anion and cation substitutions (including rare-earth elements) in various structural sites. Raman microspectroscopy revealed some specific features, inherent in molecular biomarkers (specifically, a band due to double bonds –C=C– in the central part of the polyene chain of carotenoids, which characterize cyanobacteria associated with apatite), which is a direct proof of participation of microorganisms in the formation of apatites in rocks of this deposit.
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ACKNOWLEDGMENTS
The instrumental studies were performed in the Shared Research Center of Multielement and Isotopic Studies of the Sobolev Institute of Geology and Mineralogy of the Siberian Branch of the Russian Academy of Sciences.
Funding
This study was performed within a State assignment for the Sobolev Institute of Geology and Mineralogy of the Siberian Branch of the Russian Academy of Sciences and supported by the Russian Science Foundation (project no. 18-17-00120) in the part concerning the obtainment of Nb–REE ore samples from the Tomtor deposit and their preparation for analyses, study of the geochemical features and isotopic composition of carbon and oxygen, and identification of carotenoids in the samples from boreholes 101 and 6151.
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Moroz, T.N., Palchik, N.A., Zhmodik, S.M. et al. Crystal-Chemical Features of Apatite in Carbonatites of the Tomtor Deposit (The Republic of Sakha (Yakutia), Russia): X-Ray Diffraction and Vibrational Spectroscopy Data. Crystallogr. Rep. 66, 923–930 (2021). https://doi.org/10.1134/S1063774521060225
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DOI: https://doi.org/10.1134/S1063774521060225